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Historically unprecedented global glacier decline in the early 21st century

  • Michael Zemp (a1), Holger Frey (a1), Isabelle Gärtner-Roer (a1), Samuel U. Nussbaumer (a1), Martin Hoelzle (a1) (a2), Frank Paul (a1), Wilfried Haeberli (a1), Florian Denzinger (a1), Andreas P. Ahlstrøm (a3), Brian Anderson (a4), Samjwal Bajracharya (a5), Carlo Baroni (a6), Ludwig N. Braun (a7), Bolívar E. Cáceres (a8), Gino Casassa (a9), Guillermo Cobos (a10), Luzmila R. Dávila (a11), Hugo Delgado Granados (a12), Michael N. Demuth (a13), Lydia Espizua (a14), Andrea Fischer (a15), Koji Fujita (a16), Bogdan Gadek (a17), Ali Ghazanfar (a18), Jon Ove Hagen (a19), Per Holmlund (a20), Neamat Karimi (a21), Zhongqin Li (a22), Mauri Pelto (a23), Pierre Pitte (a14), Victor V. Popovnin (a24), Cesar A. Portocarrero (a11), Rainer Prinz (a25), Chandrashekhar V. Sangewar (a26), Igor Severskiy (a27), Oddur Sigurđsson (a28), Alvaro Soruco (a29), Ryskul Usubaliev (a30) and Christian Vincent (a31)...
Abstract

Observations show that glaciers around the world are in retreat and losing mass. Internationally coordinated for over a century, glacier monitoring activities provide an unprecedented dataset of glacier observations from ground, air and space. Glacier studies generally select specific parts of these datasets to obtain optimal assessments of the mass-balance data relating to the impact that glaciers exercise on global sea-level fluctuations or on regional runoff. In this study we provide an overview and analysis of the main observational datasets compiled by the World Glacier Monitoring Service (WGMS). The dataset on glacier front variations (∼42 000 since 1600) delivers clear evidence that centennial glacier retreat is a global phenomenon. Intermittent readvance periods at regional and decadal scale are normally restricted to a subsample of glaciers and have not come close to achieving the maximum positions of the Little Ice Age (or Holocene). Glaciological and geodetic observations (∼5200 since 1850) show that the rates of early 21st-century mass loss are without precedent on a global scale, at least for the time period observed and probably also for recorded history, as indicated also in reconstructions from written and illustrated documents. This strong imbalance implies that glaciers in many regions will very likely suffer further ice loss, even if climate remains stable.

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Copyright
Copyright © International Glaciological Society 2015 This is an Open Access article, distributed under the terms of the Creative Commons Attribution license. (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited.
Corresponding author
Correspondence: Michael Zemp <michael.zemp@geo.uzh.ch>
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Complete affiliations of the WGMS National Correspondents are given in the Appendix.

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Journal of Glaciology
  • ISSN: 0022-1430
  • EISSN: 1727-5652
  • URL: /core/journals/journal-of-glaciology
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